Class #20: Friday, October 20, 2010 The C and D Climate Types Friday, October 15, 20101

The C climate types: moist, subtropical mid-latitude climates General characteristics: humid with mild winters (average temperature between 27°F and 64°F); distinct summer and winter seasons, ample precipitation Extent: on the eastern and western regions of most continents, from about 25° to 40° latitude Major types: humid subtropical (Cfa), marine (Cfb), and dry-summer subtropical or Mediterranean (Csa, Csb) Friday, October 15, 20102

Categorization of C climates CMoist with mild winters – w dry winters – s dry summers – f wet all seasons (no dry season) a summers long and hot b summers long and cool c summers short and cool See table on page 480 for details Friday, October 15, 20103

Cfa: The humid subtropical climate Found principally along the east coasts of continents 25° – 40° latitude; Southeastern section of the US, eastern China, and southern Japan. In SH, southeastern SA, Southeastern coasts of Africa and Australia Hot muggy summers: under the influence of the western side of subtropical highs, where maritime tropical air flows poleward Friday, October 15, 20104

Cfa: The humid subtropical climate Upper-level ridges produce devastating heat waves High temperatures, dew points make summer weather more uncomfortable than the tropics Winter weather can be quite changeable Little snow Adequate and well-distributed precipitation through the year Friday, October 15, 20105

Cfa: The humid subtropical climate Summer thunderstorms are common Tropical cyclones contribute to rainfall total in the US and China Winter precipitation in mid-latitude cyclones Vegetation: in southeast US, thick pine forest mixed with oak at higher latitudes Example: Mobile, Alabama Friday, October 15, 20106

Fig , p. 488

Cfb: West coast marine, or marine climate Along the west coast of most continents, from latitude 40° to about 60°. Dominated by prevailing winds from the ocean that moderate the climate (warmer winters, cooler summers) compared to farther inland. Summers are quite cool. If short, Cfc. Limited in horizontal extent by coastal mountains Friday, October 15, 20108

Cfb: West coast marine, or marine climate In western Europe, Cfb extends well inland For much of the year, low clouds, fog, drizzle Adequate precipitation in all months, from mP air masses, is light or moderate Mountains enhance precipitation Along NW coast of NA, less rain in summer, with northward migration of the subtropical high Friday, October 15, 20109

Cfb: West coast marine, or marine climate Characterized by a low annual temperature range for such high latitudes Frequent precipitation and overcast skies act to minimize daily variation in temperature Dense forest of Douglas fir where precipitation is heavy Example: Port Hardy, Vancouver Island, Canada Friday, October 15,

Fig , p. 488

Csa,b Dry-summer subtropical, or Mediterranean climate On west coasts south of the Cfb climates On the shores of the Mediterranean Sea Summer dryness more pronounced than the Cfb climates Mild (Csb) to hot (Csa) dry summers Dryness due to the sinking air in the subtropical highs and their diversion of storms poleward in summer Friday, October 15,

Csa,b Dry-summer subtropical, or Mediterranean climate During winter, subtropical highs move south, and extratropical cyclones provide rain Typically, mild wet winters Csa: interior Mediterranean (Sacramento) Csb: coastal Mediterranean (San Francisco) Friday, October 15,

Csa,b Dry-summer subtropical, or Mediterranean climate Csa – Summers are hot – Winters a little colder than Csb – Wider annual variation in temperature Csb – Upwelling keeps air cool all summer – Often shrouded in low cloud and fog – Small annual range in temperature Friday, October 15,

Fig , p. 489

Csa,b Dry-summer subtropical, or Mediterranean climate Snow is rare Land supports chaparral, a scrubby type of low-growing woody plants and trees Mediterranean Sea: summers not so dry as NA (far from subtropical high); also warmer (no upwelling) Friday, October 15,

Fig , p. 490

Cw climate type Winter dry season Associated with the winter monsoon in Asia Prevailing winds around continental High Northern India and portions of China In lower latitudes, higher altitudes keep them from being tropical because they are too cool Friday, October 15,

Fig , p. 491

Table 1, p. 492

Fig. 3, p. 492

Fig. 4, p. 493

Fig , p. 494

Fig , p. 495

Fig , p. 495